Danau Tahoe: Perbedaan antara revisi

Konten dihapus Konten ditambahkan
MelancholieBot (bicara | kontrib)
k bot Menambah: ar:بحيرة تاهو
Wadaihangit (bicara | kontrib)
melengkapi halaman dengan foto #WPWP
 
(42 revisi perantara oleh 24 pengguna tidak ditampilkan)
Baris 1:
{{Kotak info danau
| lake_name = Danau Tahoe
| image_lake = Lake Tahoe by Sentinel-2.jpg
| caption_lake = Danau Tahoe
| image_bathymetry =
| caption_bathymetry =
| coords = {{coor dm|39|6|N|120|6|W|region:US_type:waterbody}}
| type = [[sesar bongkah]]
| inflow =  
| outflow = [[Sungai Truckee]]
| catchment =
| basin_countries = [[ASAmerika Serikat]] ([[California]], [[Nevada]])
| length = 35 km
| width = 19 km
| area = 500 km²
| depth = 301 m
| max-depth = 501 m
| volume = 151 km³
| shore = 114 km
| elevation = 1.899 m
| islands =
| cities = [[South Lake Tahoe, California]]<br />[[Stateline, Nevada]]<br />[[Tahoe City, California]]
}}
'''Danau Tahoe''' adalah sebuah [[danau]] [[air tawar]] di pegunungan [[Sierra Nevada (AS)|Sierra Nevada]], yang terletak di perbatasan antara negara bagian [[California]] dan [[Nevada]] di Amerika Serikat, dekat [[Carson City, Nevada|Carson City]]. Sekitar dua pertiga garis pantainya berada di California. Di daerah ini, yang dirujuk sebagai '''Tahoe''', terdapat sejumlah tempat bermain [[resort ski|ski]] dan rekreasi tempat terbuka di musim panas.
 
Danau ini adalah yang kedua terdalam di Amerika Serikat,<ref name="Tahoe Facts">[http://tahoe.usgs.gov/facts.html Facts About Lake Tahoe] {{Webarchive|url=https://web.archive.org/web/20130411090054/http://tahoe.usgs.gov/facts.html |date=2013-04-11 }}. ''Lake Tahoe Data Clearinghouse.''</ref> yang ke-11 terdalam di dunia, dan keempat dari segi rata-rata kedalamannya.<ref name="lakes of Earth">[{{Cite web |url=http://home.comcast.net/~igpl/Lakes.html |title=Lakes of the Earth] |access-date=2003-08-04 |archive-date=2003-08-04 |archive-url=https://web.archive.org/web/20030804212041/http://home.comcast.net/~igpl/Lakes.html |dead-url=no }}</ref>
 
== Geografi ==
[[Berkas:lake-tahoe.jpg|300px|leftkiri|thumbjmpl|Pantai tenggara Danau Tahoe.]]
Danau Tahoe adalah salah satu danau terdalam (501 m), terluas (497 &nbsp;km²)¹, dan tertinggi (1898 m) di Amerika Serikat. Hanya [[Danau Crater]] di Oregon yang lebih dalam (588 m).
 
Meskipun pada sebagian besar lingkaran Danau Tahoe jalan raya melintas dalam jarak cukup dekat sehingga tepi danau dapat terlihat, beberapa bagian penting dari garis pantai California kini berada dalam lingkungan taman negara bagian atau dilindungi oleh Dinas Kehutanan Amerika Serikat. Panjang Danau Tahoe sekitar 35 &nbsp;km dan lebarnya 19 &nbsp;km. Panjang garis pantainya 116 &nbsp;km dan luas permukaannya 495 &nbsp;km².
 
Basin Danau Tahoe terbentuk oleh suatu patahan gugus geologis (normal) sekitar 2 hingga 3 juta tahun yang lalu. Patahan gugus geologis adalah suatu patahan dalam lempengan bumi yang menyebabkan gugus-gugus tanah menaik atau menurun. Gugus-gugus yang menaik menciptakan [[Carson Range]] di sebelah timur dan [[Sierra Nevada (AS)|Sierra Nevada]] di sebelah barat. Gugus-gugus yang menurun menciptakan Basin Danau Tahoe di antaranya. Sebagian dari puncak-puncak tertinggi dari Basin Danau Tahoe Basin yang terbentuk dalam proses ini adalah [[Puncak Freel]] dengan ketinggian 3320 m, Puncak Monument (3068 m) (Daerah Ski Heavenly Valley sekarang), Puncak Pyramid (3043 m) (di Gurun Desolation), dan Gunung Tallac (2967 m).
Baris 37:
 
<!--Emerald Bay State Park. A view from the east side of the lake-->
Rata-rata presipitasi berkisar antara lebih dari 140 &nbsp;cm/tahun di daerah perbatasan di sisi barat basin hingga sekitar 67 &nbsp;cm/tahun di dekat danau di sebelah timur basin. Presipitasi kebanyakan jatuh dalam bentuk salju antara November dan April, meskipun hujan badai ditambah dengan cairan salju yang cepat terjadi menyebabkan banjir yang terbesar. <!--There is a pronounced annual runoff of snowmelt in late spring and early summer, the timing of which varies from year to year. In some years, summertime monsoonal storms from the Great Basin bring intense rainfall, especially to high elevations on the east side of the basin. As the climate in the northern Sierra warms, hydrologists anticipate that an increasing fraction of the precipitation in basin will fall as rain rather than snow.
 
Vegetation in the basin is dominated by a mixed conifer forest of Jeffrey pine (P. Jeffreyi), lodgepole pine (P. murrayana), white fir (Abies concolor), and red fir (A. magnifica). The basin also contains significant areas of wet meadows and riparian areas, dry meadows, brush fields (with Arctostaphylos and Ceanothus) and rock outcrop areas, especially at higher elevations. Ceanothus is capable of fixing nitrogen, but mountain alder (Alnus tenuifolia), which grows along many of the basin’s streams, springs and seeps, fixes far greater quantities, and contributes measurably to nitrate-N concentrations in some small streams.
Baris 52:
The area around Lake Tahoe was originally inhabited by the [[Washoe (tribe)|Washoe]] tribe of [[Native Americans in the United States|Native Americans]]. Lake Tahoe was the center and heart of Washoe Indian territory, including the upper valleys of the Walker, Carson, and Truckee Rivers. They called this area "Da ow a ga", which means "edge of lake". When early pioneers came they mispronounced this word, saying "Da ow", it later evolved into what we call it today, Lake "Tahoe".. Lt. [[John C. Frémont]] and [[Kit Carson]] were the first non-indigenous people to see Lake Tahoe. It was Fremont's 2nd exploratory expedition. On February 14, [[1844]], while searching for the Bonaventura river he first sighted the lake from Red Lake Peak in what is now the Carson Pass. After arriving at Sutter's Fort he designated it Lake Bonpland, in honor of the French explorer and botanist [[Aimé Bonpland|Aimé Jacques Alexandre Bonpland]]. [[John Calhoun Johnson]], Sierra explorer and founder of "Johnson's Cutoff" (now Hwy 50), was the first white-man to see Meeks Bay and from a peak above the lake he named "[[Fallen Leaf Lake, California]]" after his Indian guide. His first employment in the west was in the government service, carrying the mail on snowshoes from Placerville to Nevada City, during which time he gave the name of Lake Bigler to that beautiful body of water now known as Lake Tahoe in honor of California’s governor [[John Bigler]]. In 1853 William Eddy, the surveyor general of California, identified Tahoe as Lake Bigler. In 1862 the [[U.S. Department of the Interior]] first introduced the name Tahoe which continued a debate about naming the lake, in which both names were used until well into the next decade. It wasn’t until 1945 that it was finally and officially named Lake Tahoe. The compromise to partition Tahoe with 2/3 to California and 1/3 to Nevada was reached when California became a state. Putting the state line right through the middle of the lake and then at 39 degrees north latitude, the stateline obliques southeasterly towards the Colorado River. Upon discovery of [[gold]] in the South Fork of the [[American River]] in [[1848]], thousands of west-bound gold seekers passed near the basin on their way to the gold fields. European civilization first made its mark in the Lake Tahoe basin with the [[1858]] discovery of the [[Comstock Lode]], a silver deposit just 15 miles (24 km) to the east in [[Virginia City, Nevada]]. From [[1858]] until about [[1890]], logging in the basin supplied large timbers to shore up the underground workings of the Comstock mines. The logging was so extensive that almost all of the native forest was cut. In [[1864]], Tahoe City was founded as a resort community for Virginia City, the first recognition of the basin’s potential as a destination resort area.
 
[[ImageBerkas:Lake tahoe and hotels 1908.jpg|thumb|250px|Lake Tahoe and hotels, 1908.]]
 
Public appreciation of the Tahoe basin grew, and during the [[Sixty-second United States Congress|1912, 1913]], and [[Sixty-fifth United States Congress|1918 Congressional session]]s, unsuccessful efforts were made to designate the basin as a [[United States National Park|national park]]. During the first half of the [[20th century]], development around the lake consisted of a few vacation homes. The post-[[World War II]] population and building boom, followed by construction of gambling casinos in the Nevada part of the basin during the mid-[[1950s]], and completion of the interstate highway links for the [[1960 Winter Olympics|1960 Squaw Valley Olympics]], resulted in a dramatic increase in development within the basin. From 1960 to 1980, the permanent resident population increased from about 10,000 to greater than 50,000, and the summer population grew from about 10,000 to about 90,000. Since the 1980s, development has slowed somewhat due to land use controls.
Baris 59:
In spite of land-use planning and export of treated sewage effluent from the basin, the lake is becoming increasingly eutrophic (richer in nutrients), with primary productivity increasing by more than 5% annually, and clarity decreasing at an average rate of 0.25 meters per year. Fine sediment, much of it resulting from land disturbance in the basin, accounts for about half of the loss in clarity.
 
Until the early 1980s, nutrient limitation studies showed that primary productivity in the lake was nitrogen-limited. Now, after a half-century of accelerated nitrogen input (much of it from direct atmospheric deposition), the lake is phosphorus-limited. Because the volume of the lake is so large (156&nbsp;km³) and its hydraulic residence time so long (about 650 years), its eutrophication may be essentially irreversible.
 
Lake Tahoe never freezes. Since 1970, it has mixed to a depth of at least 400&nbsp;m a total of 6 or 7 times. Dissolved oxygen is relatively high from top to bottom.
Baris 77:
 
== Tourist activities ==
Much of the area surrounding Lake Tahoe is devoted to the tourism industry and there are many restaurants, ski slopes and [[casino]]s catering to visitors.
 
===Winter sports===
[[ImageBerkas:Tahoe.JPG|thumbnail|right|250px|Ski slopes overlooking Lake Tahoe]]
[[ImageBerkas:IMG 7552.JPG|thumbnail|right|250px|Fallen Leaf lake (Little Tahoe) located southwest corner of the Lake Tahoe]]
During [[ski]] season, thousands of people from all over [[California]], including [[Los Angeles, California|Los Angeles]] and the [[San Francisco Bay Area]], flock to the slopes for some of the best [[skiing]] in the world. Lake Tahoe, in addition to its panoramic beauty, is well known for its [[blizzard]]s.
 
Baris 97:
*[[Homewood Ski Resort]]: a medium sized ski area on the west shore
*[[Mount Rose]]: a medium sized ski area north-east of the Lake, on Slide Mountain
 
 
For an instant overview of the locations and conditions of Tahoe ski resorts, see [http://www.skibonk.com/ski/index.jsp?query=tahoe Ski Bonk's resort map].
 
 
Scattered throughout Tahoe are public and private [[sled]] parks. Some, such as Granlibakken are equipped with [[rope tow]]s to help sledders get up the hill.
Baris 111 ⟶ 109:
Boating, the primary activity in Tahoe in the summer, is known worldwide. There are lakefront restaurants all over the Lake, most equipped with [[pier|dock]]s and [[buoys]] (See the restaurants section) There are all sorts of boating events, such as sailboat racing, firework shows over the lake, guided cruises, and more. Lake Tahoe also has its own [[Coast Guard]]
 
[[ImageBerkas:LakeTahoeFromSpace.JPG|right|thumb|225px|Lake Tahoe From Space (North is to the right)]]
 
List of Tahoe [[Marinas]]:
Baris 147 ⟶ 145:
 
== Aneka rupa ==
* Meskipun Danau Tahoe adalah sebuah danau alamiah, danau ini juga digunakan sebagai penampungan air oleh [[Distrik Irigasi Truckee-Carson]] (TCID). Permukaan danau ini dikendalikan dengan sebuah [[bendungan]] di buangan satu-satunya danau ini, yaitu [[Sungai Truckee]], di [[Tahoe City]]. Bendungan ini hanya meningkatkan kapasitas danau ini sebanyak 732.000 ''acre-feet'' dan hanya mengatur batas 6 kaki tertinggi dari danau ini.
 
* [[Bandara Internasional Reno/Tahoe]] di [[Reno, Nevada]] dan kendaraan [[Chevrolet Tahoe]] dinamai seturut dengan danau ini.
 
* Di Pantai Utara terdapat [[Cal Neva Resort]] (yang pernah dimiliki oleh [[Frank Sinatra]]) yang dilintasi garis batas antar negara bagian (bahkan juga melalui kolam renangnya).
* [[Mark Twain]] secara tidak sengaja menyebabkan kebakaran hutan di Danau Tahoe seperti yang digambarkan dalam Bab XXIII bukunya [[Roughing It]].
* Kejuaraan Vans Tahoe diadakan di [[Northstar-at-Tahoe]].
 
[[Berkas:TahoePanorama.jpg|centerpus|thumbjmpl|500px|[[Panorama]] Danau Tahoe dari Squaw Valley.]]
*[[Mark Twain]] secara tidak sengaja menyebabkan kebakaran hutan di Danau Tahoe seperti yang digambarkan dalam Bab XXIII bukunya [[Roughing It]].
 
*Kejuaraan Vans Tahoe diadakan di [[Northstar-at-Tahoe]].
 
[[Berkas:TahoePanorama.jpg|center|thumb|500px|[[Panorama]] Danau Tahoe dari Squaw Valley.]]
 
== Puncak dan gunung-gunung (dalam kaki) ==
* Gn. Tallac (9,735')
* Gn. Pluto (8,610')
* Puncak Rubicon (9,183')
* Puncak Genoa (9,150')
* Puncak Freel (10,881')
* Gn. Rose (10,778')
* Puncak Ellis (8,740')
* Puncak Scott (8,289')
* Puncak Ward (8,637')
* Puncak Dick (9,974')
* [[Puncak Maggies]] (8,699')
* Puncak Jakes (9,187')
* Puncak Monument (10,067')
* Puncak Duane Bliss (8,729')
 
== Lihat pula ==
* [[Taman Negara Emerald Bay]]
* [[Danau Mono]]
* [[Danau Clear]]
* [[Danau Pyramid]]
* [[Danau Washoe]]
* [[Danau Fallen Leaf, California]]
 
== Catatan kaki ==
Baris 187 ⟶ 181:
 
== Rujukan terpilih ==
* [http://www.tahoe.com/article/20060201/COMMUNITY07/11113035] {{Webarchive|url=https://web.archive.org/web/20100402124142/http://www.tahoe.com/article/20060201/COMMUNITY07/11113035 |date=2010-04-02 }} Tahoe.com - The naming of Tahoe's mountains
* Byron, E. R., dan C. R. Goldman, 1989. Land use and water quality in tributary streams of Lake Tahoe, California-Nevada. Jour. Environ. Qual. 18: 84-88.
* Chang, C. C. Y., J. S. Kuwabara, dan S. P. Pasilis. 1992. Phosphate and iron limitation of phytoplankton biomass in Lake Tahoe. Can. Jour. Fish. and Aquatic Sci. 49: 1206-1215.
* Coats, R. N., dan C. R. Goldman, 2001. Patterns of nitrogen transport in streams of the Lake Tahoe basin, California-Nevada. Water Resour. Res. 37: 405-415.
* Coats, R. N., J. Perez-Losada, G. Schladow, R. Richards dan C. R. Goldman. 2006. The Warming of Lake Tahoe. Climatic Change (In Press).
* Gardner, J., V., A. M. Larry, dan J. H. Clarke. 1998. The bathymetry of Lake Tahoe, California-Nevada. U.S. Geological Survey Open-File Report 98-509.
* Goldman, C. R., A. Jassby, dan T. Powell. 1989. Interannual fluctuations in primary production: meteorological forcing at two subalpine lakes. Limnol. Oceanogr. 34: 310-323.
* Goldman, C. R., A. D. Jassby, dan S. H. Hackley. 1993. Decadal, interannual, and seasonal variability in enrichment bioassays at Lake Tahoe, California-Nevada, USA. Can.J. Fish. Aquat. Sci. 50: 1489-1496.
* Hatch, L. K., J. E. Reuter, dan C. R. Goldman, 2001. Stream phosphorus transport in the Lake Tahoe Basin, 1989-1996. Environmental Monitoring and Assessment 69: 63-83.
* Jassby, A. D., C. R. Goldman, dan T. M. Powell. 1992. Trend, seasonality, cycle, and irregular fluctuations in primary productivity at Lake Tahoe, California-Nevada, USA. Hydrobiol. 246: 195-203.
* Jassby, A. D., J. E. Reuter, R. P. Axler, C. R. Goldman, dan S. H. Hackley, 1994. Atmospheric deposition of nitrogen and phosphorus in the annual nutrient load of Lake Tahoe (California-Nevada). Water Resour. Res. 30: 2207-2216.
* Jassby, A. D., C. R. Goldman dan J. E. Reuter. 1995. Long-term change in Lake Tahoe (California-Nevada, U.S.A.) and its relation to atmospheric deposition of algal nutrients. Arch. Hydrobiol. 135: 1-21.
* Jassby, A. D., C. R. Goldman, J. E. Reuter, dan R. C. Richards. 1999. Origins and scale dependence of temporal variability in the transparency of Lake Tahoe, California-Nevada. Limnol. Oceanog. 44: 282-294.
* Jassby, A., J. Reuter, dan C. R. Goldman. 2003. Determining long-term water -quality change in the presence of climate variability: Lake Tahoe (U.S.A.). Can. J. Fish. Aquat. Sci. 60: 1452-1461.
* Leonard, R. L., L. A. Kaplan, J. F. Elder, R. N. Coats, dan C. R. Goldman, 1979. Nutrient Transport in Surface Runoff from a Subalpine Watershed, Lake Tahoe Basin, California. Ecological Monographs 49: 281-310.
* Nagy, M., 2003. Lake Tahoe Basin Framework Study Groundwater Evaluation Lake Tahoe Basin, California and Nevada. U.S. Army Corps of Engineers, Sacramento, CA.
* Naslas, G. D., W. W. Miller, R. R. Blank dan G. F. Gifford, 1994. Sediment, nitrate, and ammonium in surface runoff from two Tahoe basin soil types. Water Resour. Bull. 30: 409-417.
* Richards, R. C., C. R. Goldman, E. Byron, dan C. Levitan, 1991. The mysids and lake trout of Lake Tahoe: A 25-year history of changes in the fertility, plankton, and fishery of an alpine lake. Am. Fish. Soc. Symp. 9: 30-38.
* Schuster, S., dan M. E. Grismer, 2004. Evaluation of water quality projects in the Lake Tahoe Basin. Environmental Monitoring and Assessment 90: 225-242.
 
== Pranala luar ==
{{commonscat|Lake Tahoe}}
* [http://tahoe.usgs.gov/ Lake Tahoe Data Clearinghouse] {{Webarchive|url=https://web.archive.org/web/20071028100430/http://tahoe.usgs.gov/ |date=2007-10-28 }} - USGS/Western Geographic Science Center
* [http://www.trpa.org/ Tahoe Regional Planning Agency] {{Webarchive|url=https://web.archive.org/web/20201126145318/http://www.trpa.org/ |date=2020-11-26 }}
* [http://www.rntl.net/tahoecam.htm TAHOE CAM ~Live webcam~]
* [http://www.lake-tahoe-california-hotels.com/lake-tahoe-web-cam.php Lake Tahoe]{{Pranala mati|date=Maret 2021 |bot=InternetArchiveBot |fix-attempted=yes }} Webcam from 3 Peaks Resort
* [http://terc.ucdavis.edu/ Tahoe Environmental Research Center] {{Webarchive|url=https://web.archive.org/web/20201019215140/https://tahoe.ucdavis.edu/ |date=2020-10-19 }} - UC Davis research & outreach
* [http://remote.ucdavis.edu/tahoe_location.asp Lake Tahoe REMOTE Meteorological Data Sites] {{Webarchive|url=https://web.archive.org/web/20080329183429/http://remote.ucdavis.edu/tahoe_location.asp |date=2008-03-29 }}
* [http://endeavor.des.ucdavis.edu/newcara/basin.asp?cara_id=56 Lake Tahoe Watershed] {{Webarchive|url=https://web.archive.org/web/20050126012133/http://endeavor.des.ucdavis.edu/newcara/basin.asp?cara_id=56 |date=2005-01-26 }}- California Rivers Assessment database
* [http://www.fs.fed.us/r5/ltbmu/ Lake Tahoe Basin Management Unit] - USDA Forest Service
* [http://www.flickr.com/groups/tahoe/ Lake Tahoe Photographs] - Lake Tahoe group at Flickr
* [http://www.tahoelocals.com Tahoe Locals] - Local Resource Guide
* [http://www.pbase.com/montecarloss/lake_tahoe_immigration_rally Lake Tahoe Immigration Rally Photographs]
* [http://www.keeptahoeblue.org League to Save Lake Tahoe] -environmental watchdog organization
* [http://www.tahoebaikal.org Tahoe-Baikal Institute] -international environmental organization
* [http://www.aboutlaketahoe.com/ Guide, Forums, and over 2,000 tahoe area photos] from AboutLakeTahoe.com
* [http://tahoe.usgs.gov/facts.html USGS facts about Lake Tahoe] {{Webarchive|url=https://web.archive.org/web/20130411090054/http://tahoe.usgs.gov/facts.html |date=2013-04-11 }} - PD source
<!--{{Geolinks-US-cityscale|39.09|-120.04}}-->
{{Negara bagian California}}
{{Negara bagian Nevada}}
 
[[Kategori:Basin]]
[[Kategori:Danau di Amerika Serikat]]
[[Kategori:Resort ski di Amerika Serikat]]
 
[[ar:بحيرة تاهو]]
[[bg:Тахо (езеро)]]
[[cs:Tahoe]]
[[de:Lake Tahoe]]
[[en:Lake Tahoe]]
[[eo:Lago Tahoe]]
[[es:Lago Tahoe]]
[[et:Tahoe järv]]
[[fa:دریاچه تاهو]]
[[fi:Tahoejärvi]]
[[fr:Lac Tahoe]]
[[he:אגם טאהו]]
[[it:Lago Tahoe]]
[[ja:タホ湖]]
[[nl:Lake Tahoe]]
[[no:Tahoesjøen]]
[[pl:Tahoe]]
[[ru:Тахо (озеро)]]
[[simple:Lake Tahoe]]
[[uk:Тахо]]
[[vi:Hồ Tahoe]]
[[zh:塔霍湖]]